Chvilevaite is an extremely rare sodium-bearing copper sulfide mineral primarily found in hydrothermal ore deposits. Collectors typically encounter it as small, bronzeish metallic grains associated with other sulfide minerals like sphalerite and galena.
Is this chvilevaite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch chvilevaite with a known reference. Chvilevaite sits at Mohs 3.5-4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: light yellow.
- 3Read the lusterHold the specimen under a strong light. Luster: metallic.
- 4Match the color rangeCompare against the expected color range: bronze, black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: granular aggregates, irregular grains.
Often confused with
Chvilevaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside chvilevaite
Minerals reported to co-occur with chvilevaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na(Cu,Fe,Zn)₂S₂
- Mohs hardness
- 3.5-4
- Density
- 3.94 g/cm³
- Streak
- Light yellow
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Granular aggregates, irregular grains
- Cleavage
- Perfect on {0001}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of hydrothermal origin
Where rockhounds find chvilevaite
Classic worldwide localities
- Akatui Pb–Zn deposit, Akatui, eastern Transbaikal, Russia (type locality)
Field-hunting tip
Where it forms: Of hydrothermal origin. If you start seeing sphalerite, covellite, chalcocite in float, you are in the right ground. Typical habit: granular aggregates, irregular grains. Train your eye for that shape before scanning the outcrop.








